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UPSC Prelims 2019 Q44: Geography – Atmosphere & Climatology

UPSC Prelims 2019, General Studies Paper I · Geography

Why are dewdrops not formed on a cloudy night?
  1. (a) Clouds absorb the radiation released from the Earth's surface.
  2. (b) Clouds reflect back the Earth's radiation.
  3. (c) The Earth's surface would have low temperature on cloudy nights.
  4. (d) Clouds deflect the blowing wind to ground level.

Answer: (b) Clouds reflect back the Earth's radiation.

Explanation

Why No Dew on a Cloudy Night

OptionClaimVerdictDetail
(a)Clouds absorb Earth's radiationPartially true but not the primary mechanismClouds do absorb some IR but the dominant effect is REFLECTION back to surface.
(b)Clouds reflect back Earth's radiationCORRECTCloud cover traps outgoing longwave (IR) radiation and re-radiates it back to the surface - Earth's surface stays WARMER on cloudy nights. Since the surface does not cool below the dew point, dew does not form.
(c)Earth's surface has LOW temperature on cloudy nightsFALSE (reversed)Actually surface stays WARMER, not colder, on cloudy nights (that's why dew doesn't form).
(d)Clouds deflect wind to groundIrrelevantWind deflection is unrelated to dew formation.

Answer: (b) Clouds reflect back the Earth's radiation.

Why each option is right or wrong

Key point

No dew on cloudy nights because clouds reflect outgoing longwave radiation -> surface stays warm -> doesn't reach dew point -> no condensation.

Remember

Dewdrops do not form on cloudy nights because clouds reflect back the Earth's outgoing longwave radiation, keeping the surface warmer than it would be under a clear sky. Without cooling to the dew point, water vapour does not condense into dew.

Common mistakes

Exam tip

Dew formation checklist: (i) Clear sky -> maximum longwave radiation escape -> surface cools. (ii) Calm wind -> no mixing, surface layer cools further. (iii) High humidity -> dew point reached easily. (iv) Cool surface below dew point -> condensation as dew. All four fail on cloudy, windy or dry nights.

Sources

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